2015
DOI: 10.1016/j.enconman.2015.06.049
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Effects of key factors on solar aided methane steam reforming in porous medium thermochemical reactor

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Cited by 44 publications
(6 citation statements)
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“…Similarly, these approaches and the improved Monte Carlo Ray Tracing method can also be used fairly to predict the radiative properties of the packed bed regarded as an equivalent homogeneous medium for both the semi-transparent particles and the opaque particles [82,89]. Once the radiative properties are obtained, the radiative heat exchange inside either the porous volumetric receiver or the pecked-bed PSRs can be computed by applying the typical simulation method of the RTE, such as the Rosseland approximation [15,23,[90][91][92][93][94], the P1 method [27,28,57,60,[95][96][97] and the discrete ordinates method [16,66,98,99]. Since the extinction coefficient of the porous materials is up to several hundred per meter (m −1 ) Once the radiative properties are obtained, the radiative heat exchange inside either the porous volumetric receiver or the pecked-bed PSRs can be computed by applying the typical simulation method of the RTE, such as the Rosseland approximation [15,23,[90][91][92][93][94], the P 1 method [27,28,57,60,[95][96][97] and the discrete ordinates method [16,66,98,99].…”
Section: Continuous Particle Modelmentioning
confidence: 99%
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“…Similarly, these approaches and the improved Monte Carlo Ray Tracing method can also be used fairly to predict the radiative properties of the packed bed regarded as an equivalent homogeneous medium for both the semi-transparent particles and the opaque particles [82,89]. Once the radiative properties are obtained, the radiative heat exchange inside either the porous volumetric receiver or the pecked-bed PSRs can be computed by applying the typical simulation method of the RTE, such as the Rosseland approximation [15,23,[90][91][92][93][94], the P1 method [27,28,57,60,[95][96][97] and the discrete ordinates method [16,66,98,99]. Since the extinction coefficient of the porous materials is up to several hundred per meter (m −1 ) Once the radiative properties are obtained, the radiative heat exchange inside either the porous volumetric receiver or the pecked-bed PSRs can be computed by applying the typical simulation method of the RTE, such as the Rosseland approximation [15,23,[90][91][92][93][94], the P 1 method [27,28,57,60,[95][96][97] and the discrete ordinates method [16,66,98,99].…”
Section: Continuous Particle Modelmentioning
confidence: 99%
“…Once the radiative properties are obtained, the radiative heat exchange inside either the porous volumetric receiver or the pecked-bed PSRs can be computed by applying the typical simulation method of the RTE, such as the Rosseland approximation [15,23,[90][91][92][93][94], the P1 method [27,28,57,60,[95][96][97] and the discrete ordinates method [16,66,98,99]. Since the extinction coefficient of the porous materials is up to several hundred per meter (m −1 ) Once the radiative properties are obtained, the radiative heat exchange inside either the porous volumetric receiver or the pecked-bed PSRs can be computed by applying the typical simulation method of the RTE, such as the Rosseland approximation [15,23,[90][91][92][93][94], the P 1 method [27,28,57,60,[95][96][97] and the discrete ordinates method [16,66,98,99]. Since the extinction coefficient of the porous materials is up to several hundred per meter (m −1 ) orders, there is no difference in the results of the radiative heat exchange solved by these methods.…”
Section: Continuous Particle Modelmentioning
confidence: 99%
“…There is growing interest in hydrogen as a promising energy carrier, because of its high calorific value and pollution-free character as fuel. [1] One of the synthesis routes of hydrogen production is steam reforming using natural gas, alcohols, biogas, etc. as feedstock.…”
Section: Introductionmentioning
confidence: 99%
“…However, elemental hydrogen is not found on earth and must be chemically separated from one of its compounds such as water or methane. Commercially, methane steam reforming (MSR) is used to convert fossil methane to hydrogen gas and carbon monoxide (as syngas) at high temperature, providing over half of global hydrogen production. The reaction is endergonic and endothermic, requiring high energy input at high temperature. Together with MSR, the water-gas shift (WGS) reaction takes places, where carbon monoxide reacts with water to form carbon dioxide and hydrogen. …”
Section: Introductionmentioning
confidence: 99%